One practice used to control irrigation-induced erosion amends irrigat
ion furrow inflows with water-soluble, anionic polyacrylamide (PAM) at
low concentrations (0.25-10 mg L(-1)). Researchers wish to determine
the fate of PAM, once added to furrow water streams. We developed and
tested an instrumented flocculation test for quantifying PAM concentra
tion in irrigation water. A kaolinite mineral standard is mixed with a
PAM-amended water sample, agitated, then placed in a spectrophotomete
r. The PAM concentration in the suspension was correlated with settlin
g-related transmittance changes. One highly correlated (r = 0.91-0.98)
parameter, the time needed to initiate suspension clearing (clarity-s
hift inflection, CSI), was used as the procedure endpoint. The procedu
re was sensitive to variations in the amount of kaolinite added, and s
ample volume, water salinity, and original sediment content. A 10% cha
nge in these factors altered measured CSIs by 10 to 50%. The sediment
affected CSI by increasing the sample's dissolved organic C concentrat
ion. The procedure detected as little as 0.1 mg L(-1) PAM dissolved in
irrigation water; in samples containing > 4 mt settled sediment per l
iter, the PAM detection limit was approximately 0.25 mg L(-1). Precisi
on ranged from +/- 0.06 to 0.11 mg L(-1) for 0 to 2.5 mg L(-1) PAM and
+/- 0.39 to 0.86 mg L(-1) for 2.5 to 10.0 mg L(-1) PAM. The PAM conce
ntration in runoff from irrigated furrows equaled that of the inflow s
tream after 3 h continuous treatment at 10 mg L(-1). The CSI test prov
ides a simple and accurate method of determining polyacrylamide in sur
face waters.